The Ecology, Biogeochemistry, and Optical Properties of Coccolithophores

Coccolithophores are major contributors to phytoplankton communities and ocean biogeochemistry and are strong modulators of the optical field in the sea. New discoveries are changing paradigms about these calcifiers. A new role for silicon in coccolithophore calcification is coupling carbonate and s...

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Published inAnnual review of marine science Vol. 10; no. 1; pp. 71 - 98
Main Author Balch, William M
Format Journal Article
LanguageEnglish
Published United States Annual Reviews 03.01.2018
Annual Reviews, Inc
Subjects
Alkalinity
Backscattering
Biogeochemistry
Calcification
Calcification, Physiologic
carbon cycling
Carbon dioxide
Carbonates
Carbonates - chemistry
coccolithophores
Coccoliths
Coupling (molecular)
Detection
Ecology
Iron
Mixotrophy
Modulators
Morphometry
nutrients
ocean optics
Oceans and Seas
Optical Phenomena
Optical properties
Phosphorus
Phytoplankton
Phytoplankton - chemistry
Phytoplankton - physiology
Primary production
Remote sensing
Satellites
Seawater - chemistry
Silicon
Silicon - chemistry
Temperature
trace metals
carbon cycling
trace metals
mixotrophy
phytoplankton
ocean optics
calcification
coccolithophores
nutrients
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Abstract Coccolithophores are major contributors to phytoplankton communities and ocean biogeochemistry and are strong modulators of the optical field in the sea. New discoveries are changing paradigms about these calcifiers. A new role for silicon in coccolithophore calcification is coupling carbonate and silicon cycles. Phosphorus and iron play key roles in regulating coccolithophore growth. Comparing molecular phylogenies with coccolith morphometrics is forcing the reconciliation of biological and geological observations. Mixotrophy may be a possible life strategy for deep-dwelling species, which has ramifications for biological pump and alkalinity pump paradigms. Climate, ocean temperatures, and pH appear to be affecting coccolithophores in unexpected ways. Global calcification is approximately 1-3% of primary productivity and affects CO 2 budgets. New measurements of the backscattering cross section of coccolithophores have improved satellite-based algorithms and their application in case I and case II optical waters. Remote sensing has allowed the detection of basin-scale coccolithophore features in the Southern Ocean.
AbstractList Coccolithophores are major contributors to phytoplankton communities and ocean biogeochemistry and are strong modulators of the optical field in the sea. New discoveries are changing paradigms about these calcifiers. A new role for silicon in coccolithophore calcification is coupling carbonate and silicon cycles. Phosphorus and iron play key roles in regulating coccolithophore growth. Comparing molecular phylogenies with coccolith morphometrics is forcing the reconciliation of biological and geological observations. Mixotrophy may be a possible life strategy for deep-dwelling species, which has ramifications for biological pump and alkalinity pump paradigms. Climate, ocean temperatures, and pH appear to be affecting coccolithophores in unexpected ways. Global calcification is approximately 1-3% of primary productivity and affects CO2 budgets. New measurements of the backscattering cross section of coccolithophores have improved satellite-based algorithms and their application in case I and case II optical waters. Remote sensing has allowed the detection of basin-scale coccolithophore features in the Southern Ocean.
Coccolithophores are major contributors to phytoplankton communities and ocean biogeochemistry and are strong modulators of the optical field in the sea. New discoveries are changing paradigms about these calcifiers. A new role for silicon in coccolithophore calcification is coupling carbonate and silicon cycles. Phosphorus and iron play key roles in regulating coccolithophore growth. Comparing molecular phylogenies with coccolith morphometrics is forcing the reconciliation of biological and geological observations. Mixotrophy may be a possible life strategy for deep-dwelling species, which has ramifications for biological pump and alkalinity pump paradigms. Climate, ocean temperatures, and pH appear to be affecting coccolithophores in unexpected ways. Global calcification is approximately 1-3% of primary productivity and affects CO 2 budgets. New measurements of the backscattering cross section of coccolithophores have improved satellite-based algorithms and their application in case I and case II optical waters. Remote sensing has allowed the detection of basin-scale coccolithophore features in the Southern Ocean.
Coccolithophores are major contributors to phytoplankton communities and ocean biogeochemistry and are strong modulators of the optical field in the sea. New discoveries are changing paradigms about these calcifiers. A new role for silicon in coccolithophore calcification is coupling carbonate and silicon cycles. Phosphorus and iron play key roles in regulating coccolithophore growth. Comparing molecular phylogenies with coccolith morphometrics is forcing the reconciliation of biological and geological observations. Mixotrophy may be a possible life strategy for deep-dwelling species, which has ramifications for biological pump and alkalinity pump paradigms. Climate, ocean temperatures, and pH appear to be affecting coccolithophores in unexpected ways. Global calcification is approximately 1-3% of primary productivity and affects CO budgets. New measurements of the backscattering cross section of coccolithophores have improved satellite-based algorithms and their application in case I and case II optical waters. Remote sensing has allowed the detection of basin-scale coccolithophore features in the Southern Ocean.
Coccolithophores are major contributors to phytoplankton communities and ocean biogeochemistry and are strong modulators of the optical field in the sea. New discoveries are changing paradigms about these calcifiers. A new role for silicon in coccolithophore calcification is coupling carbonate and silicon cycles. Phosphorus and iron play key roles in regulating coccolithophore growth. Comparing molecular phylogenies with coccolith morphometrics is forcing the reconciliation of biological and geological observations. Mixotrophy may be a possible life strategy for deep-dwelling species, which has ramifications for biological pump and alkalinity pump paradigms. Climate, ocean temperatures, and pH appear to be affecting coccolithophores in unexpected ways. Global calcification is approximately 1–3% of primary productivity and affects CO 2 budgets. New measurements of the backscattering cross section of coccolithophores have improved satellite-based algorithms and their application in case I and case II optical waters. Remote sensing has allowed the detection of basin-scale coccolithophore features in the Southern Ocean.
Author Balch, William M
AuthorAffiliation Bigelow Laboratory for Ocean Sciences, East Boothbay, Maine 04544, USA; email
bbalch@bigelow.org
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Keywords carbon cycling
trace metals
mixotrophy
phytoplankton
ocean optics
calcification
coccolithophores
nutrients
Language English
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Snippet Coccolithophores are major contributors to phytoplankton communities and ocean biogeochemistry and are strong modulators of the optical field in the sea. New...
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SubjectTerms Alkalinity
Backscattering
Biogeochemistry
Calcification
Calcification, Physiologic
carbon cycling
Carbon dioxide
Carbonates
Carbonates - chemistry
coccolithophores
Coccoliths
Coupling (molecular)
Detection
Ecology
Iron
Mixotrophy
Modulators
Morphometry
nutrients
ocean optics
Oceans and Seas
Optical Phenomena
Optical properties
Phosphorus
Phytoplankton
Phytoplankton - chemistry
Phytoplankton - physiology
Primary production
Remote sensing
Satellites
Seawater - chemistry
Silicon
Silicon - chemistry
Temperature
trace metals
Title The Ecology, Biogeochemistry, and Optical Properties of Coccolithophores
URI http://dx.doi.org/10.1146/annurev-marine-121916-063319
https://www.ncbi.nlm.nih.gov/pubmed/29298138
https://www.proquest.com/docview/2014963233
https://search.proquest.com/docview/1984752353
Volume 10
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